Osl dating of sediments from deserts in northern china,

Quaternary Science Reviews 11, An Outline on Chinese Deserts. At that time, it was supported by Manas River in the osl dating of sediments from deserts in northern china Fig. Origin and derived courses of eolian dust quartz deposited during marine isotope stage 2 in East Asia, suggested by ESR signal intensity.

OSL samples were taken either by hammering stainless steel tubes cm long with 5-cm diameter into an exposed sedimentary section site 1or by taking block samples site 3. Spatial and temporal characteristics of dust storms in China and its surrounding regions, — A review of current research on TL dating of loess.

The sedimentary break indicates that large-scale erosion may have occurred in the area. Stepwise advance of the Mn Us Desert since late Pliocene: Science in China Series D italian online dating scams, It is therefore important to understand the spatial extent and the timing of neotectonic activities in the area, before a detailed paleoenvironmental change can be inferred.

It is noted that the evolution of Manas Lake was controlled not only by climate change, but also neotectonic activities Wang, ; Mu et al.

As it was too hard for hammering stainless steel tube into the section, block samples were taken directly instead. Using the OSL single-aliquot regenerative-dose protocol with quartz extracted from building materials in retrospective dosimetry.

At present, Manas Lake is an intermittent lake occasionally supported by Manas River, as well as groundwater discharge Zhang and Li, ; Yao and Li, Mineral separation was then carried out on a selected grain size fraction using sodium polytungstate solution of densities 2.

Geophysical Research Letters 35, An exposed vertical sedimentary section was found Fig. AfterMana River can occasionally reach Manas Lake again.

Earth and Planetary Science Letters A continuous OSL scanning method for analysis of radiation depth-dose profiles in bricks. An Introduction to Optical Dating. Difference in luminescence sensitivity of coarse-grained quartz from deserts of northern China. Loess and the Environment. However, radiocarbon dating requires carbon-rich materials which are not common in Manas Lake sediments, and may suffer from old carbon contamination e.

Journal of Geophysical Research-AtmospheresD10 Quaternary Geochronology 1, Provenance of loess material and formation of loess deposits on the Chinese Loess Plateau.

The large lake was a wandering lake, originally formed due to tectonic subsidence in the western part of Junggar Basin in the early Pleistocene Wang, This layer is further underlain by relatively wet, yellowish brown coarse sand with some sub-rounded gravels at the bottom of the section.

Wang also found a sedimentary break in his sampling section of the upper paleoshoreline in the southeastern side MS-2B of Fig. OSL samples were collected from each of the three sandy layers Fig. In Chinese Li, S. Understanding past changes of the lake is important in predicting future hydrological changes, as well as managing water resources in the region.

Optical dating of young modern sediments using quartz — results from a selection of deposition of depositional-environments. Later, Wang focused on dating young, late Holocene sediments of Manas Lake. Fluvial transport as a natural luminescence sensitiser of quartz. Geochronometria 44, 1; Despite such an arid condition, Manas Lake once had a lake surface area of km2 60—70 km long and 10—20 km wide and an average water depth of 6 m in Zhang and Li, Variations in OSL components from quartz from Japan sea sediments and the possibility of reconstructing provenance.

Catena Supplement 9, Provenance, transport and characteristics of modern aeolian dust in western Gansu Province, China, and interpretation of the Quaternary loess record. Also, previous studies on older sediments in the area only focused on northwestern side of the lake Fan et al.

The bottom of the section is made of yellowish grey, poorly sorted fluvial gravels dominantly pebbles and granuleswhich is more than 2 m thick. These two periods correspond to the relatively warm and humid period during marine isotope stage 5 MIS 5 and late MIS 3 respectively. Based on radiocarbon dating, Rhodes et al.

The signals Lx and Tx were obtained from the integrated photon counts in the initial 0. At this period, site A was at or near a paleoshoreline environment. The relatively coarse grain size of sand indicates a near-shore environment, with a paleo-current dominantly flowing to the center of the lake as indicated by cross-bedding.

Quaternary Geochronology 5, It is therefore necessary to take samples again from the southeastern side for OSL dating, in order to allow comparison between the two sides of the lake at similar elevation.

The relatively fine-grain nature of the sand suggests an offshore shallow lacustrine environment. They were likely deposited in recent flooding events. Compositions of heavy minerals in Northeastern China sandlands and provenance analysis.

Oxygen isotope calibration of the onset of ice-rafting and history of glaciation in the northeast Atlantic. The elevation shown is in meters above sea level.

Radiation Measurements 44, Optically stimulated luminescence dating as a tool for calculating sedimentation rates in Chinese loess: Geological Society of America Bulletin In Chinese Yang, X. Due to intensified agricultural activities which used water intensively, the Manas River was cut off at its lower course and it could not reach Manas Lake Cheng et al.

The brownish color indicates an oxidizing environment. In Chinese Ma, L. Quaternary Science Reviews 16, It also helps to determine the time when relatively wet episodes occurred in the lake area.